메뉴 건너뛰기




Volumn 33, Issue 10, 2006, Pages

Excess pore pressures within subducting sediments: Does the proportion of accreted versus subducted sediments matter?

Author keywords

[No Author keywords available]

Indexed keywords

DEFORMATION; PORE PRESSURE; SEDIMENTS; SEISMOLOGY; THICKNESS MEASUREMENT;

EID: 33745857249     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2006GL025737     Document Type: Article
Times cited : (7)

References (17)
  • 1
    • 0003134188 scopus 로고
    • Density, porosity, and compaction of sedimentary rocks
    • Athy, L. F. (1930), Density, porosity, and compaction of sedimentary rocks, AAPG Bull., 14, 1-24.
    • (1930) AAPG Bull. , vol.14 , pp. 1-24
    • Athy, L.F.1
  • 2
    • 0027061287 scopus 로고
    • A simplified analysis of parameters controlling dewatering in accretionary prisms
    • Bekins, B. A., and S. J. Dreiss (1992), A simplified analysis of parameters controlling dewatering in accretionary prisms, Earth Planet. Sci. Lett., 109, 275-287.
    • (1992) Earth Planet. Sci. Lett. , vol.109 , pp. 275-287
    • Bekins, B.A.1    Dreiss, S.J.2
  • 3
    • 0029414070 scopus 로고
    • Episodic and constant flow models for the origin of low-chloride waters in a modern accretionary complex
    • Bekins, B. A., A. M. McCaffrey, and S. J. Dreiss (1995), Episodic and constant flow models for the origin of low-chloride waters in a modern accretionary complex, Water Resour. Res., 31, 3205-3216.
    • (1995) Water Resour. Res. , vol.31 , pp. 3205-3216
    • Bekins, B.A.1    McCaffrey, A.M.2    Dreiss, S.J.3
  • 4
    • 0020684081 scopus 로고
    • Mechanics of fold and thrust belts and accretionary wedges
    • Davis, D. M., J. Suppe, and F. A. Dahlen (1983), Mechanics of fold and thrust belts and accretionary wedges, J. Geophys. Res., 88, 1153-1172.
    • (1983) J. Geophys. Res. , vol.88 , pp. 1153-1172
    • Davis, D.M.1    Suppe, J.2    Dahlen, F.A.3
  • 5
    • 33744928150 scopus 로고    scopus 로고
    • Characterization of excess pore pressures at the toe of the Nankai accretionary complex, Ocean Drilling Program sites 1173, 1174, and 808: Results of one-dimensional modeling
    • B04103 doi:10.1029/2004JB003572
    • Gamage, K., and E. Screaton (2006), Characterization of excess pore pressures at the toe of the Nankai accretionary complex, Ocean Drilling Program sites 1173, 1174, and 808: Results of one-dimensional modeling, J. Geophys. Res., 111, B04103, doi:10.1029/2004JB003572.
    • (2006) J. Geophys. Res. , vol.111
    • Gamage, K.1    Screaton, E.2
  • 6
    • 0028193105 scopus 로고
    • A physical explanation for the positioning of the depth to the top of overpressures in shale-dominated sequences in the Gulf Coast basin, United States
    • Mello, U. T., G. D. Karner, and R. N. Anderson (1994), A physical explanation for the positioning of the depth to the top of overpressures in shale-dominated sequences in the Gulf Coast basin, United States, J. Geophys. Res., 99, 2775-2789.
    • (1994) J. Geophys. Res. , vol.99 , pp. 2775-2789
    • Mello, U.T.1    Karner, G.D.2    Anderson, R.N.3
  • 7
    • 84879884609 scopus 로고    scopus 로고
    • Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stress
    • Moore, J. C., and D. M. Saffer (2001), Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stress, Geology, 29, 183-186.
    • (2001) Geology , vol.29 , pp. 183-186
    • Moore, J.C.1    Saffer, D.M.2
  • 8
    • 0022768149 scopus 로고
    • Groundwater flow in low-permeability environments
    • Neuzil, C. E. (1986), Groundwater flow in low-permeability environments, Water Resour. Res., 22, 1163-1195.
    • (1986) Water Resour. Res. , vol.22 , pp. 1163-1195
    • Neuzil, C.E.1
  • 9
    • 0032506815 scopus 로고    scopus 로고
    • Episodic fluid flow in the Nankai accretionary complex: Timescale, geochermstry, flow rates, and fluid budget
    • Saffer, D. M., and B. A. Bekins (1998), Episodic fluid flow in the Nankai accretionary complex: Timescale, geochermstry, flow rates, and fluid budget, J. Geophys. Res., 103, 30,351-30,370.
    • (1998) J. Geophys. Res. , vol.103
    • Saffer, D.M.1    Bekins, B.A.2
  • 10
    • 84874995482 scopus 로고    scopus 로고
    • Hydrologic controls on the morphology and mechanics of accretionary wedges
    • Saffer, D. M., and B. A. Bekins (2002), Hydrologic controls on the morphology and mechanics of accretionary wedges, Geology, 30, 271-274.
    • (2002) Geology , vol.30 , pp. 271-274
    • Saffer, D.M.1    Bekins, B.A.2
  • 11
    • 16344389403 scopus 로고    scopus 로고
    • Permeability of underthrust sediments at the Costa Rican subduction zone: Scale dependence and implications for dewatering
    • L02302 doi:10.1029/2004GL021388
    • Saffer, D. M., and A. W. McKiernan (2005), Permeability of underthrust sediments at the Costa Rican subduction zone: Scale dependence and implications for dewatering, Geophys. Res. Lett., 32, L02302, doi:10.1029/2004GL021388.
    • (2005) Geophys. Res. Lett. , vol.32
    • Saffer, D.M.1    McKiernan, A.W.2
  • 12
    • 18344384958 scopus 로고    scopus 로고
    • Fluid expulsion and overpressure development during initial subduction at the Costa Rica convergent margin
    • Screaton, E. J., and D. M. Saffer (2005), Fluid expulsion and overpressure development during initial subduction at the Costa Rica convergent margin, Earth Planet. Sci. Lett., 233(3-4), 361-374.
    • (2005) Earth Planet. Sci. Lett. , vol.233 , Issue.3-4 , pp. 361-374
    • Screaton, E.J.1    Saffer, D.M.2
  • 13
    • 0024525240 scopus 로고
    • Hydrogeological modeling of porous flow in the Oregon accretionary prism
    • Shi, Y., C. Y. Wang, W.-T. Hwang, and R. von Huene (1989), Hydrogeological modeling of porous flow in the Oregon accretionary prism, Geology 17(4), 231-323.
    • (1989) Geology , vol.17 , Issue.4 , pp. 231-323
    • Shi, Y.1    Wang, C.Y.2    Hwang, W.-T.3    von Huene, R.4
  • 14
    • 33744903424 scopus 로고    scopus 로고
    • Hydrogeologic responses to three-dimensional temperature variability, Costa Rica subduction margin
    • B04403 doi:10.1029/2004JB003436
    • Spinelli, G. A., D. M. Saffer, and M. B. Underwood (2006), Hydrogeologic responses to three-dimensional temperature variability, Costa Rica subduction margin, J. Geophys. Res., 111, B04403, doi:10.1029/ 2004JB003436.
    • (2006) J. Geophys. Res. , vol.111
    • Spinelli, G.A.1    Saffer, D.M.2    Underwood, M.B.3
  • 15
    • 0034962996 scopus 로고    scopus 로고
    • Modeling consolidation and dewatering near the toe of the northern Barbados accretionary complex
    • Stauffer, P., and B. A. Bekins (2001), Modeling consolidation and dewatering near the toe of the northern Barbados accretionary complex, J. Geophys. Res., 106, 6369-6384.
    • (2001) J. Geophys. Res. , vol.106 , pp. 6369-6384
    • Stauffer, P.1    Bekins, B.A.2
  • 16
    • 0026307889 scopus 로고
    • Observations at convergent margins concerning sediment subduction, subduction erosion, and the growth of continental crust
    • Von Huene, R., and D. W. Scholl (1991), Observations at convergent margins concerning sediment subduction, subduction erosion, and the growth of continental crust, Rev. Geophys., 29(3), 279-316.
    • (1991) Rev. Geophys. , vol.29 , Issue.3 , pp. 279-316
    • Von Huene, R.1    Scholl, D.W.2
  • 17
    • 0003239605 scopus 로고
    • A finite element simulation model for saturated-unsaturated, fluid density-dependent groundwater flow with energy transport or chemically-reactive single-species solute transport
    • 4369
    • Voss, C. I. (1984), A finite element simulation model for saturated-unsaturated, fluid density-dependent groundwater flow with energy transport or chemically-reactive single-species solute transport, U.S. Geol. Surv. Water Resour. Invest., 84-4369, 409 pp.
    • (1984) U.S. Geol. Surv. Water Resour. Invest. , vol.84 , pp. 409
    • Voss, C.I.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.